Zobrazeno 1 - 6
of 6
pro vyhledávání: '"D. S. Battisti"'
Publikováno v:
Geophysical Research Letters, Vol 51, Iss 8, Pp n/a-n/a (2024)
Abstract The observed partitioning of poleward heat transport between atmospheric and oceanic heat transports (AHT and OHT) is compared to that in coupled climate models. Model ensemble mean poleward OHT is biased low in both hemispheres, with the la
Externí odkaz:
https://doaj.org/article/228971917d8146db8b02267525066457
Publikováno v:
Geophysical Research Letters, Vol 50, Iss 20, Pp n/a-n/a (2023)
Abstract Arctic warming under increased CO2 peaks in winter, but is influenced by summer forcing via seasonal ocean heat storage. Yet changes in atmospheric heat transport into the Arctic have mainly been investigated in the annual mean or winter, wi
Externí odkaz:
https://doaj.org/article/a264a687956d4a8380b94ea66b0faae9
Publikováno v:
Weather and Climate Dynamics, Vol 2, Pp 777-794 (2021)
The efficacy of Euro-Atlantic circulation regimes for estimating wintertime climate anomalies (precipitation and surface temperature) over Europe is assessed. A comparison of seasonal climate reconstructions from two different regime frameworks (clus
Externí odkaz:
https://doaj.org/article/d714b4a70b0342969f0164bd3b995074
Publikováno v:
Climate of the Past, Vol 5, Iss 3, Pp 489-502 (2009)
Using four different climate models, we investigate sea level pressure variability in the extratropical North Atlantic in the preindustrial climate (1750 AD) and at the Last Glacial Maximum (LGM, 21 kyrs before present) in order to understand how cha
Externí odkaz:
https://doaj.org/article/6655de27944a4bc9871320221cb40861
Publikováno v:
Climate Dynamics. 59:2181-2196
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cf9ccaa7d2b13757d742b7398fcd0759
https://doi.org/10.1007/s00382-022-06203-6
https://doi.org/10.1007/s00382-022-06203-6
Publikováno v:
Journal of Climate. 24:5192-5194
Penny et al. recently showed that the midwinter suppression in storminess over the western and central Pacific Ocean is due to a reduction in the number and amplitude of “seed” disturbances entering the Pacific storm track from midlatitude Asia.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cfe806a224079060ad2ca6ed5bf24aa8
https://doi.org/10.1175/2011jcli4187.1
https://doi.org/10.1175/2011jcli4187.1